River terraces are geomorphic features that signify former floodplain levels created by the ongoing processes of erosion and deposition. When a stream vertically erodes into its own floodplain, it creates terraces, which can be made of bedrock or alluvial deposits. The presence of multiple terraces at varying heights indicates the history of the river's activity over time. When river terraces exist at the same elevation on both sides of a river, they are categorized as paired terraces. This remarkable feature offers insights into the history of river evolution and the geomorphic alterations in the landscape.